Plates:a section of the lithosphere that slowly moves carrying pieces of the crust Scientific Theory:a well tested theory Plate Tectonics:the geological theory that states that pieces of the Earth's lithoshere are in constant movement
due to convection currents in the mantle Faults:breaks in the Earth's crust where rocks have slipped passed each other Transform Boundary:a place where two plates slipped pass each other, in opposite directions Divergent Boundary:a place where two plates diverge, or move apart Rift Valley:a deep valley that forms along a divergent boundary Convergent Boundary:a place where two plates collide,come together,or converge
Outline
Theory of Plate Motion
Wilson combined sea-floor speading and continental drift into a single theory
his theory states that the Earth's lithosphere is broken into pieces called plates
Theory includes that the plates are driven by convection currents in the mantle
Plate boundaries
plates meet at a boundary
there are three different boundaries
transform,divergent,convergent
The Continents' Slow Dance
plates move slowly
2.5 cm a year, about same rate as fingernails grow
about 260 million years ago, continents were combined into pangaea
Table of Contents
Chapter 1.5
Vocabulary
Plates:a section of the lithosphere that slowly moves carrying pieces of the crust
Scientific Theory:a well tested theory
Plate Tectonics:the geological theory that states that pieces of the Earth's lithoshere are in constant movement
due to convection currents in the mantle
Faults:breaks in the Earth's crust where rocks have slipped passed each other
Transform Boundary:a place where two plates slipped pass each other, in opposite directions
Divergent Boundary:a place where two plates diverge, or move apart
Rift Valley:a deep valley that forms along a divergent boundary
Convergent Boundary:a place where two plates collide,come together,or converge
Outline
Theory of Plate Motion
Plate boundaries
The Continents' Slow Dance
- plates move slowly
- 2.5 cm a year, about same rate as fingernails grow
- about 260 million years ago, continents were combined into pangaea
- they broke at 225 million years ago
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